地球化学背景的英文

• geochemical background

• "背景"英文翻译    background; backdrop; settin ...
• "区域地球化学背景" 英文翻译 :    regional geochemical background
• "化学背景" 英文翻译 :    chemical background; chemical ground
• "水化学背景值" 英文翻译 :    hydrogeochemical background value
• "引言与化学背景" 英文翻译 :    introduction and chemical background
• "地球化学" 英文翻译 :    genochemistry; geochemistry; geochimica; geokhimiya
• "地球化学表" 英文翻译 :    geochemical table
• "地球化学的" 英文翻译 :    geochemical
• "地球化学家" 英文翻译 :    geochemist
• "地球化学面" 英文翻译 :    geochemical surface
• "地球化学区" 英文翻译 :    geochemical province; geochemical zone; geochemicalprovince
• "地球化学圈" 英文翻译 :    geochemical sphere
• "地球化学省" 英文翻译 :    geochemical province
• "地球化学图" 英文翻译 :    geochemical map; geochemicalmap
• "地球化学相" 英文翻译 :    elemental facies; geochemical facies; geochemical phase; geochemicalfacies
• "地球化学晕" 英文翻译 :    geochemical halo
• "地球化学障" 英文翻译 :    geochemical barriers
• "地球化学酌" 英文翻译 :    geochemical process; geochemicalproce
• "地球化学族" 英文翻译 :    geochemical family
• "电地球化学" 英文翻译 :    electrogeochemistry
• "核地球化学" 英文翻译 :    nuclear geochemistry; nulcear geochemistry
• "犬地球化学" 英文翻译 :    biocaningeochemistry
• "水地球化学" 英文翻译 :    water geochemistry
• "液地球化学" 英文翻译 :    hydrogeochemistry
• "比较地球化学" 英文翻译 :    comparative geochemistry

• Geochemical background and element distribution in soil in chengdu , sichuan
  四川成都土壤地球化学背景及元素分布
• Based on these , the enrichment mode of the geochemical elements and their distribution in space are discussed and the anomaly lower limit can be obtained and then the geochemical backgrounds 、 regional anomalies and local anomalies are distinguished
  在此基础上，分析了元素的成矿富集规律和空间分布特征，确定了区域异常和局部异常的异常下限，划分了地球化学背景、区域异常和局部异常。
• Focuses on maolan karst forest nature reserve in guizhou province , the study presents contrasts on characteristics of element geochemistry , resident flora and species diversity in two kinds of karst environments where bedrocks are respectively made up of pure limestone and pure dolomite
  该区生态系统不断退化，生物多样性大量丧失，不同喀斯特地球化学背景下植被恢复的速度与成林性质存在明显差异。
• This study choosed arc view gis by way of foundation platform and developed the function modules for region geophysics and geochemistry ( for example hydrological function and background analyst for region geochemistry and transformation for potency field and transformation of map projection and correlation analyst and grid data treating and inserter for kriging and trend and so on ) except using the basic functions of arc view gis ( e . g . neighbour analyst and spatial data treating and surface analyst and model constructor and so on )
  本论文选择arcviewgis作为基础平台，除利用arcviewgis的基本功能(如邻域分析、空间数据处理、表面分析、模型构造器等)外，开发了适合于区域地球物理地球化学综合解释的功能模块，如水文功能、区域地球化学背景分析、位场变换、地图投影变换、相关场分析、栅格数据处理、 kriging及trend插值器等。
• The results shows that the community richness , species diversity indices and evenness of tree layer and shrub layer share the same order , of which is higher in pure limestone region than that of in pure dolomite region , but it reverse in herb layer ; the coefficient of similarity is considerably low between all plots , while species turnover rate is quite high among the plots and is higher in dolomite region than that of in limestone ; in different karst regions , karst processing leads to niches diversity characterized by special morphologies and special element geochamical features , and therefore affect the dynamic and features of plant communities
  我们在最有代表性之一的贵州茂兰喀斯特森林保护区选取纯灰岩和纯白云岩两种岩性的喀斯特环境，对其元素地球化学特征及其中原生性植物群落的相异性和物种多样性进行了对比，结果发现：不同岩性区域多样性：乔木层和灌木层为纯灰岩区纯白云岩区，草本层为纯白云岩区纯灰岩区，总体上纯灰岩区的高于纯白云岩区的；各样地间的相似性系数都很低，相同岩性类型内的明显高于不同岩性类型之间的相似度；物种周转率高，且白云岩区高于石灰岩区，种类组成差异明显；喀斯特区可溶岩地球化学背景通过喀斯特作用导致特殊的地形条件与元素地球化学特征，并引起局部小生境的分异从而影响植物群落特征。
• In the link party of qinling - qiliang - kunlun belt , the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin . the bayan har basin thought to be the preexistence of the songpan - garze belt , is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic . the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ) , then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic
  在秦祁昆仑结合部研究中，加强和突出了精细的岛弧盆分析和造山作用关系的研究，探讨了秦、祁、昆结合部多岛弧盆特征；通过巴颜喀拉地区沉积特征，沉积体的空间展布和形态，面式物源供给方式，矿物成分和地球化学背景分析，其沉积盆地属性总体上反映出一个从过渡地壳-洋壳基础上发育起来的周缘前陆盆地的发展和演化过程。